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Planar Velocity Distribution of Viscous Debris Flow at Jiangjia Ravine, Yunnan, China: A Field Measurement Using Two Radar Velocimeters

机译:云南省江家沟壑区粘性泥石流的平面速度分布:利用两个雷达测速仪的现场测量

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摘要

Characteristics of planar velocity distribution of viscous debris flow were analyzed using the measured data at Jiangjia Ravine, Yunnan, China. The velocity data were measured through using two radar velocimeters. The cross-sectional mean velocities were calculated and used to examine Kang et al's (2004) relationship, which was established for converting the flow velocity at river centerline measured by a radar velocimeter into the mean velocity based on the stop-watch method. The velocity coefficient, K, defined by the ratio of the mean velocity to the maximum velocity, ranges from 0.2 to 0.6. Kang et al's (2004) relationship was found being inapplicable to flows with K smaller than 0.43. This paper contributes to show the complexity of the planarvelocity distribution of viscous debris flows and the applicability of Kang et al's relationship.
机译:利用云南江家沟沟的实测数据分析了泥石流的平面速度分布特征。通过使用两个雷达测速仪测量速度数据。计算断面平均速度,并将其用于检验Kang等人(2004年)的关系,该关系是根据秒表方法将雷达速度计测得的河流中心线处的流速转换为平均速度而建立的。由平均速度与最大速度之比定义的速度系数K介于0.2到0.6之间。 Kang等人(2004年)的关系不适用于K小于0.43的流。本文有助于说明粘性泥石流平面速度分布的复杂性以及Kang等人关系的适用性。

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